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黄土坡面侵蚀产沙时空演变的REE示踪技术研究

Study on spatial-temporal process of soil loss on loess slope surface by rare earth element tracers technology

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【作者】 薛亚洲刘普灵杨明义琚彤军

【Author】 XUE Ya-zhou~(1,2), LIU Pu-ling~1, YANG Ming-yi~1,JU Tong-jun~1(1.State Key Laboratory of Soil Erosion And Dryland Farming on Loess Plateau ,Institute of Soil and Water Conservation, CAS and MWR, Yangling 712100, China;2.Chinese Academy of Land and Resources Economics, Beijing 101149, China)

【机构】 中国科学院水利部水土保持研究所土壤侵蚀与旱地农业国家重点实验室中国科学院水利部水土保持研究所土壤侵蚀与旱地农业国家重点实验室 陕西杨凌 712100中国国土资源经济研究院北京 101149陕西杨凌 712100陕西杨凌 712100

【摘要】 室内交叉布设不同的稀土氧化物,通过人工模拟次降雨,在同一试验条件下,对坡面侵蚀沿顺坡方向和深度方向的演变过程同时展开研究。结果表明:REE示踪技术对定量研究土壤侵蚀具有较高的精度;降雨前期,片蚀与细沟侵蚀发育程度基本相当;后期细沟侵蚀占据坡面侵蚀的主导地位,其侵蚀平均加速度和平均侵蚀率分别是片蚀的15倍、9倍;试验结束,细沟侵蚀占据坡面总侵蚀的90%;本试验条件下,坡面下1/3区域为侵蚀活跃带。

【Abstract】 By placing different rare earth elements (REE) in different soil depth and different section across one slope in an indoor plot, one simulated rainfall was applied to study the spatial-temporal process both of depth and section erosion across one slope plot simultaneously. The results indicated that the REE tracer technology has high precision to quantify the spatial-temporal process of soil erosion; In earlier rainfall course, the development degree of sheet and rill erosion was general equation; Otherwise in the following course, the rill erosion was dominant in the total erosion, its average erosion acceleration and the average erosion rate was 15 and 9 times of sheet erosion, respectively; In the end of experiment, the rill erosion took up 90% of total erosion amount; The section of slope bottom occupying about 1/3 slope area was active erosion segment in this experiment.

【基金】 国家自然科学基金资助项目(40471079);国家自然科学重点基金资助项目(40335050);中国科学院知识创新重要方向项目(KZCX3 SW 422)~~
  • 【文献出处】 水科学进展 ,Advances In Water Science , 编辑部邮箱 ,2005年02期
  • 【分类号】S157.1
  • 【被引频次】22
  • 【下载频次】315
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